Articles | Volume 12, issue 10
Nat. Hazards Earth Syst. Sci., 12, 3139–3150, 2012
https://doi.org/10.5194/nhess-12-3139-2012

Special issue: Weather-related hazards and risks in agriculture

Nat. Hazards Earth Syst. Sci., 12, 3139–3150, 2012
https://doi.org/10.5194/nhess-12-3139-2012

Research article 19 Oct 2012

Research article | 19 Oct 2012

Assessment of remotely sensed drought features in vulnerable agriculture

N. R. Dalezios*,1, A. Blanta1, and N. V. Spyropoulos2 N. R. Dalezios et al.
  • 1Laboratory of Agrometeorology, Department of Agriculture, Ichthyology & Aquatic Environment, School of Agricultural Sciences, University of Thessaly, Volos, Greece
  • 2Department of Natural Resources Development and Agricultural Engineering, Agricultural University of Athens, Athens, Greece
  • *currently at: Senior Research Associate, Institute of Technology & Management of Agricultural Ecosystems (ITEMA)/Center for Research and Technology, Thessaly (CE.RE.TE.TH), First Industrial Area, Volos, Greece

Abstract. The growing number and effectiveness of Earth observation satellite systems, along with the increasing reliability of remote sensing methodologies and techniques, present a wide range of new capabilities in monitoring and assessing droughts. A number of drought indices have been developed based on NOAA-AVHRR data exploiting the remote sensing potential at different temporal scales. In this paper, the remotely sensed Reconnaissance Drought Index (RDI) is employed for the quantification of drought. RDI enables the assessment of hydro-meteorological drought, since it uses hydrometeorological parameters, such as precipitation and potential evapotranspiration. The study area is Thessaly, central Greece, which is a drought-prone agricultural region characterized by vulnerable agriculture. Several drought features are analyzed and assessed by using monthly RDI images over the period 1981–2001: severity, areal extent, duration, periodicity, onset and end time. The results show an increase in the areal extent during each drought episode and that droughts are classified into two classes, namely small areal extent drought and large areal extent drought, respectively, lasting 12 or 13 months coinciding closely with the hydrological year. The onset of large droughts coincides with the beginning of the hydrological year, whereas the onset of small droughts is in spring. During each drought episode, the maximum occurs usually in the summer and they all last until the end of the hydrological year. This finding could justify an empirical prognostic potential of drought assessment.

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